Conodont evidence for the age of the Radomir Formation in the Vlahina and Konjava Mountains (southwest Bulgaria)

Pages: 
pp. 79-85
Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria
Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria
Abstract: 

Key sections of the Radomir Formation in the Vlahina and Konjava Mountains have been systematically sampled and studied for conodonts. The conodonts determined prove a Middle Triassic age for the most of the section. The Illyrian substage of the Anisian and the Fassanian and Longobardian substage of the Ladinian are proven by the presence of the zones Pridaella cornuta R.Z., Pridaella excentrica A.Z., Pridaella bakalovi R.Z., and Paragondolella foliata R.Z.

К. Будуров, А. Вапцарова. Конодонтные доказательства о возрасте Радомирской свиты во Влахина-планине и Конявска-планине (Юго-Западная Болгария). В исследованных породах Радомирской свиты во Влахина-планине и Конявска-планине найдены конодонты, которые доказывают среднетриасовый возраст для большей ее части.  Посредством зон Pridaella cornuta R.Z., Pridaella excentrica A.Z., Pridaella bakalovi R.Z., and Paragondolella foliata R.Z. доказаны иллирийский подъярус аниза и фасанский и лонгобардский подъярусы ладина.

DOI: 
10.52321/GeolBalc.24.1.79

VOLUME 24 (1)/February 1994

Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria

Department of Geology and Paleontology, Geological-Geographical Faculty, Sofia University "St. Kliment Ohridski", 1000 Sofia

Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria
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Geological Institute, Bulgarian Academy of Sciences, 1113 Sofia, Bulgaria

National Museum of Natural History, Bulgarian Academy of Sciences, 1000 Sofia, Bulgaria